The holocenic evolution of a stretch of an eastern italian alpine valley
The morphological evolution of a stretch of an alpine valley located in the Eastern Italian Alps is described. This has been conditioned by a great alluvial fan that was formed as a consequence of interconnected events, deriving from large rockfalls which occurred in the late glacial period at the h...
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Veröffentlicht in: | Earth surface processes and landforms 1995-12, Vol.20 (8), p.747-757 |
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Format: | Artikel |
Sprache: | eng |
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